首页> 外文期刊>Applied and Environmental Microbiology >Effects of co-occurring aromatic hydrocarbons on degradation of individual polycyclic aromatic hydrocarbons in marine sediment slurries.
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Effects of co-occurring aromatic hydrocarbons on degradation of individual polycyclic aromatic hydrocarbons in marine sediment slurries.

机译:共同芳烃对海洋沉积物浆料中各多环芳烃劣化的影响。

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Rates of polycyclic aromatic hydrocarbon (PAH) degradation and mineralization were influenced by preexposure to alternate PAHs and a monoaromatic hydrocarbon at relatively high (100 ppm) concentrations in organic-rich aerobic marine sediments. Prior exposure to three PAHs and benzene resulted in enhanced [14C]naphthalene mineralization, while [14C]anthracene mineralization was stimulated only by benzene and anthracene preexposure. Preexposure of sediment slurries to phenanthrene stimulated the initial degradation of anthracene. Prior exposure to naphthalene stimulated the initial degradation of phenanthrene but had no effect on either the initial degradation or mineralization of anthracene. For those compounds which stimulated [14C]anthracene or [14C]naphthalene mineralization, longer preexposures (2 weeks) to alternative aromatic hydrocarbons resulted in an even greater stimulation response. Enrichment with individual PAHs followed by subsequent incubation with one or two PAHs showed no alteration in degradation patterns due to the simultaneous presence of PAHs. The evidence suggests that exposure of marine sediments to a particular PAH or benzene results in the enhanced ability of these sediments to subsequently degrade that PAH as well as certain other PAHs. The enhanced degradation of a particular PAH after sediments have been exposed to it may result from the selection and proliferation of specific microbial populations capable of degrading it. The enhanced degradation of other PAHs after exposure to a single PAH suggests that the populations selected have either broad specificity for PAHs, common pathways of PAH degradation, or both.
机译:多环芳烃(PAH)降解和矿化的速率受到在富含有氧的有氧海洋沉积物中相对高(100ppm)浓度的交替PAHs和单芳烃中的替代PAHS和单芳烃。在三种PAHS和苯的暴露之前导致增强的[14C]萘矿化,而仅通过苯和蒽培训刺激[14C]蒽矿化。沉积物浆液对菲恩的预先筛选刺激了蒽的初始降解。在萘前暴露于萘刺激菲苯乙烯的初始降解,但对蒽的初始降解或矿化无效。对于刺激[14C]蒽或[14℃]萘矿化的那些化合物,替代芳族烃的更长的预×(2周)导致更大的刺激反应。与单个PAH的富集,随后与一个或两个PAH一起孵育,由于PAHs的同时存在,没有促进降解模式的变化。证据表明,暴露海洋沉积物对特定的PAH或苯导致这些沉积物的增强能力随后降解PAH以及某些其他PAH。在沉积物之后的特定PAH的增强降解已经暴露于它可能是由能够降解其降解的特异性微生物种群的选择和增殖产生。暴露于单个PAH后,其他PAHs的增强降解表明,所选择的群体对PAHS的群体具有广泛的特异性,PAH降解的常见途径或两者。

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